Matches in SemOpenAlex for { <https://semopenalex.org/work/W2886110621> ?p ?o ?g. }
- W2886110621 endingPage "504" @default.
- W2886110621 startingPage "494" @default.
- W2886110621 abstract "This study presents 1) the results of a stable isotope and subfossil Cladocera analyses of lacustrine sediments from Maliszewskie Lake (E Poland) and next 2) different reaction of the lake environments depending on the lake's localization. Maliszewskie Lake is located in North Podlasie Lowland ca. 30 km to the south of the Vistulian ice sheet limit. The approximately 4.80-m-thick sediments (Maliszewo I profile) are mainly comprised of calcareous gyttja covered by peat and organic detritus gyttja. Pollen analysis documents that the sediments accumulated from the Late Glacial (Allerød period) to recent times. Based on the results of stable isotope and subfossil Cladocera analyses of sediments, the lake environmental changes were reconstructed. A positive trend in δ18O and δ13C values documents a gradual climatic warming. The fluctuations of the oxygen isotopic values suggest the multiple oscillation of water level due to a change in the evaporation/precipitation ratio. The subfossil cladoceran fauna in the Maliszewo I profile is represented by 21 species belonging to five families. Three zones of Cladocera development were distinguished. The Cladocera species indicate the initial oligotrophic status of the lake and its subsequent increase of trophic status. Currently, Maliszewskie Lake is a very shallow, declining reservoir. The initial period of its existence probably saw its maximal depth. In presented studies we compared our results with data from three other sites documenting the reaction of the lake environment during the Late Glacial and Holocene transformation. At that time we observed different reactions to the climate amelioration. In the northern, postglacial lakes, the Holocene warming at first provoked an input cold melting water characterized by more negative oxygen isotope values and then a rise in water temperature. In the lakes further away from the glaciation border (periglacial lakes), the increase in water temperature, documented by e.g. more positive oxygen isotopic immediately occurred. The climate warming is commonly manifested by a significant increase of number of species and individuals of Cladocera." @default.
- W2886110621 created "2018-08-22" @default.
- W2886110621 creator A5032212200 @default.
- W2886110621 creator A5079536259 @default.
- W2886110621 date "2018-12-01" @default.
- W2886110621 modified "2023-10-14" @default.
- W2886110621 title "Reaction of the lake environment to the Holocene warming depending on the distance to the maximum extent of the Vistulian ice sheet" @default.
- W2886110621 cites W1504160556 @default.
- W2886110621 cites W1511995191 @default.
- W2886110621 cites W1578339091 @default.
- W2886110621 cites W1965164453 @default.
- W2886110621 cites W1971907424 @default.
- W2886110621 cites W1977038202 @default.
- W2886110621 cites W1977341063 @default.
- W2886110621 cites W1978056511 @default.
- W2886110621 cites W1980843372 @default.
- W2886110621 cites W1981225366 @default.
- W2886110621 cites W1987983531 @default.
- W2886110621 cites W1990783861 @default.
- W2886110621 cites W1993681650 @default.
- W2886110621 cites W1999430005 @default.
- W2886110621 cites W2000431240 @default.
- W2886110621 cites W2001604947 @default.
- W2886110621 cites W2004569583 @default.
- W2886110621 cites W2005649253 @default.
- W2886110621 cites W2008281306 @default.
- W2886110621 cites W2009073988 @default.
- W2886110621 cites W2012821805 @default.
- W2886110621 cites W2013024602 @default.
- W2886110621 cites W2013777620 @default.
- W2886110621 cites W2023464588 @default.
- W2886110621 cites W2028556967 @default.
- W2886110621 cites W2032201066 @default.
- W2886110621 cites W2045105922 @default.
- W2886110621 cites W2049832246 @default.
- W2886110621 cites W2059997981 @default.
- W2886110621 cites W2070157067 @default.
- W2886110621 cites W2071184501 @default.
- W2886110621 cites W2081261658 @default.
- W2886110621 cites W2098195774 @default.
- W2886110621 cites W2105691658 @default.
- W2886110621 cites W2120637384 @default.
- W2886110621 cites W2124038226 @default.
- W2886110621 cites W2138834810 @default.
- W2886110621 cites W2160850801 @default.
- W2886110621 cites W2911528385 @default.
- W2886110621 cites W4249751050 @default.
- W2886110621 cites W881784775 @default.
- W2886110621 cites W1979535233 @default.
- W2886110621 cites W1998034280 @default.
- W2886110621 doi "https://doi.org/10.1016/j.catena.2018.07.033" @default.
- W2886110621 hasPublicationYear "2018" @default.
- W2886110621 type Work @default.
- W2886110621 sameAs 2886110621 @default.
- W2886110621 citedByCount "5" @default.
- W2886110621 countsByYear W28861106212019 @default.
- W2886110621 countsByYear W28861106212020 @default.
- W2886110621 countsByYear W28861106212022 @default.
- W2886110621 countsByYear W28861106212023 @default.
- W2886110621 crossrefType "journal-article" @default.
- W2886110621 hasAuthorship W2886110621A5032212200 @default.
- W2886110621 hasAuthorship W2886110621A5079536259 @default.
- W2886110621 hasConcept C100970517 @default.
- W2886110621 hasConcept C111368507 @default.
- W2886110621 hasConcept C127313418 @default.
- W2886110621 hasConcept C140345934 @default.
- W2886110621 hasConcept C151730666 @default.
- W2886110621 hasConcept C15739521 @default.
- W2886110621 hasConcept C158836135 @default.
- W2886110621 hasConcept C174110039 @default.
- W2886110621 hasConcept C205649164 @default.
- W2886110621 hasConcept C26099304 @default.
- W2886110621 hasConcept C2776200160 @default.
- W2886110621 hasConcept C2778208666 @default.
- W2886110621 hasConceptScore W2886110621C100970517 @default.
- W2886110621 hasConceptScore W2886110621C111368507 @default.
- W2886110621 hasConceptScore W2886110621C127313418 @default.
- W2886110621 hasConceptScore W2886110621C140345934 @default.
- W2886110621 hasConceptScore W2886110621C151730666 @default.
- W2886110621 hasConceptScore W2886110621C15739521 @default.
- W2886110621 hasConceptScore W2886110621C158836135 @default.
- W2886110621 hasConceptScore W2886110621C174110039 @default.
- W2886110621 hasConceptScore W2886110621C205649164 @default.
- W2886110621 hasConceptScore W2886110621C26099304 @default.
- W2886110621 hasConceptScore W2886110621C2776200160 @default.
- W2886110621 hasConceptScore W2886110621C2778208666 @default.
- W2886110621 hasFunder F4320322511 @default.
- W2886110621 hasLocation W28861106211 @default.
- W2886110621 hasOpenAccess W2886110621 @default.
- W2886110621 hasPrimaryLocation W28861106211 @default.
- W2886110621 hasRelatedWork W1990803640 @default.
- W2886110621 hasRelatedWork W2004056635 @default.
- W2886110621 hasRelatedWork W2079467660 @default.
- W2886110621 hasRelatedWork W2093089000 @default.
- W2886110621 hasRelatedWork W2479901346 @default.
- W2886110621 hasRelatedWork W27956163 @default.
- W2886110621 hasRelatedWork W4284714095 @default.
- W2886110621 hasRelatedWork W4294323191 @default.